Nordenskiöld斯匹次卑尔根岛冰川的冰储量及其在过去几十年的变化

IF 0.7 Q4 GEOSCIENCES, MULTIDISCIPLINARY Led i Sneg-Ice and Snow Pub Date : 2019-03-20 DOI:10.15356/2076-6734-2019-1-23-38
I. Lavrentiev, A. Glazovsky, Y. Macheret, V. Matskovsky, A. Y. Muravyev
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These two glaciers account for 67% of the total measured volume (10,034 km3) of the 16 glaciers. A nonlinear least-squares method was used to estimate ice reserves in all 202 glaciers from data on the volume and area of 16 glaciers. The relation between volume V and area A of the  glaciers (V–A scaling) was obtained as the ratio V = 0.03637A1,283 with 95%‑th confidence intervals of the coefficients с and γ, (0.02303–0,4971) and (1.184–1.381), respectively. This made possible to calculate total volume of 202 glaciers as of 2002-2008 state using data from RGI v.6.0, and that prove to be equal to 32.89 (16.75–56.63) km3. 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引用次数: 3

摘要

在1999年和2010-2013年获得了Nordenskiöld陆地(斯瓦尔巴群岛)上16个冰川的厚度和面积数据。利用这些数据确定冰川的体积,并以幂函数V = cAγ的形式建立体积V与面积A之间的统计局部关系(V - A标度),进而计算出该地区所有202座冰川的总冰体积及其在1936年至2002-2008年期间的变化。16条冰川总面积为129.9±0.35 km2,其中14条冰川面积在0.2 ~ 8.1 km2之间。最大的两个冰川Fridtjof和West grenjord的面积分别为17.5和47.3 km2,约占16个冰川总面积的50% (64.8 km2)。这两个冰川占16个冰川总测量体积(10034 km3)的67%。利用16个冰川的体积和面积数据,采用非线性最小二乘法估算了202个冰川的冰储量。冰川体积V与面积A之间的关系(V - A标度)为比值V = 0.03637A1,283,系数r(0.02303 - 0,4971)和γ(1.184-1.381)的95%置信区间分别为(0.02303 - 0,4971)和(1.184-1.381)。利用RGI v.6.0的数据计算2002-2008年状态下202个冰川的总积,结果为32.89 (16.75-56.63)km3。为了验证这一估计,我们对选定的43个冰川采用了bootstrapping方法,并通过顺序使用大冰川和小冰川的数据来计算体积。根据估算,202座冰川的总体积为30.34 km3, 95%置信区间为15.42 ~ 44.27 km3,略小于基于16座冰川实测数据的非线性最小二乘法计算的体积。尽管在估算Nordenskiöld Land的202个冰川的总体积时误差较大(平均误差在- 49%到+84%之间),但所获得的数据用于评估该地区冰川总体积在不同时间间隔内的相对变化。从1936年到1990年(54 a),所有冰川的总面积从738.1 km2减少到546.7 km2,总积从49,205 km2减少到34,857 km2。1990-2002-2008年(~15 a)期间,总面积从546.7 km2变化到507.9 km2,总体积从34.857 km2变化到32.890 km2。1936 - 1990年期间的体积减少率为- 0.266 km3/年,1990-2002-2008年期间为- 0.131 km3/年,整个研究期间(自1936年至2002-2008年)的体积减少率为- 0.236 km3/年。第一阶段的平均质量平衡为−0.372 m w.e./年,第二阶段为−0.224 m w.e./年,整个时期的平均质量平衡为−0.342 m w.e./年。
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Reserve of ice in glaciers on the Nordenskiöld Land, Spitsbergen, and their changes over the last decades
Data on thickness and area of 16 glaciers on the Nordenskiöld Land (Svalbard) were obtained in 1999 and 2010–2013. These data were used to determine volume of the glaciers and to establish statistical local relationship between the volume V and the area A (V–A scaling) in the form of the power function V = cAγ, and then to calculate the total ice volume of all 202 glaciers in this area and its changes during the period since 1936 to 2002–2008. The total area of 16 glaciers was 129.9±0.35 km2, 14 of which had areas from 0.2 to 8.1 km2. The two largest ones, the Fridtjof and the West Grenfjord, had the areas 17.5 and 47.3 km2, respectively, and thus occupied about 50% (64.8 km2) of the total area of 16 glaciers. These two glaciers account for 67% of the total measured volume (10,034 km3) of the 16 glaciers. A nonlinear least-squares method was used to estimate ice reserves in all 202 glaciers from data on the volume and area of 16 glaciers. The relation between volume V and area A of the  glaciers (V–A scaling) was obtained as the ratio V = 0.03637A1,283 with 95%‑th confidence intervals of the coefficients с and γ, (0.02303–0,4971) and (1.184–1.381), respectively. This made possible to calculate total volume of 202 glaciers as of 2002-2008 state using data from RGI v.6.0, and that prove to be equal to 32.89 (16.75–56.63) km3. To verify this estimation, we applied the bootstrapping method for chosen 43 glaciers and calculated the volume by means of sequential use of data for large and smaller glaciers. According to this estimate, the total volume of 202 glaciers amounted to 30.34 km3 with a 95% confidence interval of 15.42–44.27 km3, that turned out to be slightly smaller than the volume calculated by nonlinear least squares method basing on measurements on 16 glaciers. Despite the large error (on the average, from −49% to +84%) in estimating the total volume of 202 glaciers in the Nordenskiöld Land, the data obtained were used for assessment of relative changes in the total volume of glaciers in this area over different time intervals. During the period from 1936 to1990 (54 years), the total area of all glaciers reduced from 738.1 to 546.7 km2, and the total volume decreased from 49,205 to 34,857 km3. Similar results for the period 1990–2002–2008 (~15 years) are the total area changes from 546.7 to 507.9 km2 and their total volume - from 34.857 to 32.890 km3. The rate of decrease of the volume for the period 1936–1990 was equal to −0.266 km3/year, for the period 1990–2002–2008 – minus 0.131 km3/year, and as a whole for the studied period (since 1936 to 2002–2008) – minus  0.236 km3/year. The average mass balance in the first period was equal to −0.372 m w.e./year, in the second one −0.224 m w.e./year, and for the whole time −0.342 m w.e./year. 
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来源期刊
Led i Sneg-Ice and Snow
Led i Sneg-Ice and Snow GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
1.50
自引率
42.90%
发文量
11
审稿时长
8 weeks
期刊介绍: The journal was established with the aim of publishing new research results of the Earth cryosphere. Results of works in physics, mechanics, geophysics, and geochemistry of snow and ice are published here together with geographical aspects of the snow-ice phenomena occurrence in their interaction with other components of the environment. The challenge was to discuss the latest results of investigations carried out on Russia’s territory and works performed by Russian investigators together with foreign colleagues. Editorial board works in collaboration with Glaciological Association that is professional community of specialists in glaciology from all republics of the Former Soviet Union which are now new independent states. The journal serves as a platform for the presentation and discussion of new discoveries and results which help to elucidate the state of the Earth’s cryosphere and the characteristics of the evolution of the snow-ice processes and phenomena under the current conditions of rapid climate change.
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СТОХАСТИЧЕСКОЕ МОДЕЛИРОВАНИЕ ПОЛЕЙ СПЛОЧЁННОСТИ ЛЕДЯНОГО ПОКРОВА ДЛЯ ОЦЕНКИ УСЛОВИЙ ПЛАВАНИЯ ПО ТРАССЕ СЕВЕРНОГО МОРСКОГО ПУТИ ЭВОЛЮЦИЯ ОЗЁР У ЛЕДНИКА ДЖИКИУГАНКЕЗ (СЕВЕРНОЕ ПРИЭЛЬБРУСЬЕ) В 1957-2020 ГГ. С УЧЁТОМ ПОДЗЕМНЫХ КАНАЛОВ СТОКА ВЛИЯНИЕ РЕЖИМА СНЕЖНОГО ПОКРОВА НА АГРОНОМИЧЕСКИЕ РИСКИ РАЗВИТИЯ РОЗОВОЙ СНЕЖНОЙ ПЛЕСЕНИ ВЛИЯНИЕ ЗЕМЛЕТРЯСЕНИЯ 1988 Г. НА ОЛЕДЕНЕНИЕ И РЕЛЬЕФ МАССИВА ЦАМБАГАРАВ (ЗАПАДНАЯ МОНГОЛИЯ) БАЛАНС ЛЬДА В СЕВЕРНОМ ЛЕДОВИТОМ ОКЕАНЕ В 1979-2019 ГГ. (ПО ДАННЫМ МОДЕЛИРОВАНИЯ)
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